| | c41a-0294 in fm06 (Site not responding. Last check: 2007-11-02) |
 | | An additional indicator of basal properties, the basal roughness of ice sheets, may be an indicator of crustal geology and glacial modification, as well as a controlling parameter on ice dynamics and subglacial hydrology. For the Siple Coast ice streams, Fourier analysis of > 5 kilometer morphology (Siegert et al. |
 | | On the Greenland Ice Sheet, the fraction of surface melt that moves downslope varies from zero at the top of the percolation facies to one near and below the equilibrium line altitude (ELA), and is important for determination of the surface mass balance of the ice sheet. |
 | | Downslope meltwater movement is also a source for surface lakes and slush basins, and it is thought that these lakes and their associated hydraulic network are one source of englacial and subglacial water, which may cause acceleration of the ice sheet. |
| www.agu.org /cgi-bin/SFgate/SFgate?&listenv=table&multiple=1&range=1&directget=1&application=fm06&database=/data/epubs/wais/indexes/fm06/fm06&maxhits=200&="C41A-0294" (12058 words) |